This article has been reviewed according to Science X's editorial process and policies. Editors have highlighted the following attributes while ensuring the content's credibility: Lakes may cover only a small fraction of Earth's surface, but new research suggests they play a bigger role in regulating the planet's climate than previously recognized. By reflecting sunlight back into space when covered in snow and ice, lakes in the Northern Hemisphere have a stronger cooling effect than the surrounding land.
Sarah Cooley of Duke University and colleagues say their results highlight an overlooked part of Earth's climate system that could be better represented in climate models, which scientists use to understand how the planet responds to changing environmental conditions. Snow and ice play an important role in regulating Earth's temperature because their ability to reflect sunlight helps limit the amount of solar energy absorbed by the planet, producing a cooling effect known as the cryosphere radiative effect. However, snow and ice do not cover the landscape uniformly, and the way they behave can vary depending on the underlying surface.
Lakes, for example, can retain snow and ice differently from the surrounding land, potentially influencing how much sunlight is reflected back into space over the course of a year. To investigate this, the team analyzed 22 years of satellite observations, comparing seasonal snow cover and the amount of sunlight reflected by lakes and nearby land across the Northern Hemisphere. The analysis, published in Geophysical Research Letters, found that lakes have a substantially greater cooling effect per unit of area than the surrounding land: −14.4 watts per square meter over lakes, compared with −8.2 watts per square meter over land.
This difference means lakes contribute more to the reflection of sunlight than their relatively small surface area might suggest. The effect was particularly pronounced in boreal forests, which are dominated by coniferous trees and stretch across large parts of northern North America, Europe and Asia. In these regions, lakes can account for more than a quarter of the cooling effect from snow and ice.
The researchers also found that lakes' contribution becomes particularly important in late spring, when snow and ice are beginning to disappear from the landscape. Two main factors help explain why lakes have a stronger cooling effect than nearby land. The first is that snow tends to melt earlier on land, meaning the ground begins absorbing more sunlight while nearby lakes remain covered in reflective snow and ice.
The second is that snow-covered lakes reflect a greater proportion of incoming sunlight than snow-covered land, which scientists refer to as having a higher albedo. Together, these differences mean lakes can continue reflecting sunlight at a time when the surrounding landscape has already begun to absorb more of the sun's energy. This is particularly significant during the transition from winter to spring, when the amount of snow and ice across the Northern Hemisphere changes rapidly.
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